Volcanoes are the weak parts of the earth's crust; there is not one in

full activity which does not present alternative series of increase or

lessening. The cone rises gradually until by degrees it is obstructed

with lava, then a sudden fall destroys it and hollows a new crater,

sometimes larger and deeper than the first. Many such occurrences have

been described, but none can equal in importance the gigantic fall

which formed the Bay of Santorini. All the central part must have given

way, and been suddenly ingulfed, leaving but a narrow border of land,

through the northern part of which the sea has dashed to fill up the

hollow. Instead of a mountain three thousand feet high, there is a bay

of immense depth, surrounded by precipitous rocks, close to which ships

can anchor.

This violent catastrophe must have taken place when man was on the

island; and the event must have been sudden, since the remains prove

that there was no time to move away or to displace anything in the

houses. The eruption of pumice-stone has preceded the sinking of the

cone, for the tufa which covers the downs is cut through by subjacent

streams of lava; nor does it seem to have been preceded by any violent

earthquakes, as in that case the houses found in Therasia would have

been demolished and the walls no longer standing. This is remarkable,

as the construction of the buildings proves that the island was subject

to them; the pieces of wood inserted in the walls seeming to be for no

other object than to prevent the disastrous effects of such a shaking.

This custom is still in use among all the islands of the Archipelago.

From the abundance of wood used in the houses, the island must in those

days have been well supplied with timber. The olive-tree grew freely,

and barley was the commonest of the cereals. Probably too the climate

was different. The vine does not seem to have been there; still less

was it the only plant cultivated, as now, at Santorini. The population

were husbandmen, understanding how to grind barley in mills and make

it into bread; how to press oil from olives, to bring up cattle,

and to weave stuffs. Yet the great abundance of utensils of lava,

obsidian, and flint, without any metals, shews that theirs was the age

of stone, when the use of metals was unknown. The blocks of stones

at the angles of the house at Therasia and the column standing near,

indicate considerable skill in the workmen, when the kind of tools they

used is taken into consideration; whilst the vases of pottery-ware are

remarkable for their elegance of form.

It only remains to consider how many years ago it is since this great

eruption took place. The data are vague, but geologists have tried

to make some approximation. It is well known that after any violent

catastrophe the subterranean forces seem to be exhausted; the periods

of repose in a volcano are proportional to the previous energy. About

one hundred and ninety-six years before Christ there is the record of

an eruption, which raised in the centre of the bay a small islet called

Palæa Kameni. After the Christian era, frequent slight emissions only

served to increase the size of the island, and during the middle ages

there was a period of calm. In the fifteenth century the excitement

again burst forth, raising reefs both inside and outside the bay. The

second duration of rest was about ten centuries; so that to the first,

according to its intensity, there may be calculated at least twice that

time; thus the formation of the bay was perhaps two thousand years B.C.

Historical records furnish more positive teaching, as the bay certainly

existed fifteen hundred years B.C. It was at this epoch that the

islands of the Greek Archipelago were invaded by the Phœnicians. This

nation occupied Therasia and Santorini, as the many ruins still to be

found testify, and they are built on the top of the pumice-stone. But

the great eruption must have been long before that, since thick beds

of pebbles and shells, from fifteen to twenty yards deep, lie on the

tufa; and geologists know well, from the habitual slowness of this

raising of the soil, that it corresponds to many centuries. There was

also a population on the islands differing from those who were buried

in the ashes, and from the Phœnicians. The latter knew the use of

bronze, and introduced it on all the shores of the Mediterranean. Most

likely we may place the great event during the early days of Egyptian

civilisation, which some historians compute to be four or five thousand

years ago. The primitive population present no trace of the influence

which that nation exerted, and with which commerce would have placed

them in frequent relations.

* * * * *

The Conductors of CHAMBERS'S JOURNAL beg to direct the attention of

CONTRIBUTORS to the following notice:

_1st._ All communications should be addressed to the 'Editor,

339 High Street, Edinburgh.'

_2d._ To insure the return of papers that may prove ineligible,

postage-stamps should in every case accompany them.

_3d._ MANUSCRIPTS should bear the author's full _Christian_ name,

surname, and address, legibly written.

_4th._ MS. should be written on one side of the leaf only.

_5th._ Poetical offerings should be accompanied by an envelope,

stamped and directed.

_Unless Contributors comply with the above rules, the Editor cannot

undertake to return ineligible papers._

* * * * *

Printed and Published by W. & R. CHAMBERS, 47 Paternoster Row, LONDON,

and 339 High Street, EDINBURGH.

* * * * *

_All Rights Reserved._

Chambers's Journal of Popular Literature, Science, and Art, No. 727, December 1, 1877 · 第 4 / 4 段